MATERIALS 兴 HIENGE& ENGIEERING ELSEVIER Materials Science and Engineering A 438-440(2006)55-63 www.elsevier.com/locate/msea Multi-scale phase field approach to martensitic transformations Yunzhi Wang,, Armen G Khachatur a Department of Materials Science and Engineering. The Ohio State University, Columbus, OH 43210, USA b Department of Ceramic and Materials Engineering. Rutgers University, 607 Taylor Road, Piscataway, NJ08854, USA Received 18 August 2005: received in revised form 17 March 2006: accepted 17 April 2006 Because of its flexibility in treating complex geometries and topological changes, the phase field method has been used widely in modeling microstructural evolution during various phase transformations, grain growth and, most recently, plastic deformations. We review formulations and applications of the method in the context of martensitic transformations(MTs). Examples are chosen to illustrate the capabilities of the method at both mesoscopic and microscopic length scales. At the mesoscopic level we present simulation predictions on structural configurations of critical nuclei generated by homogeneous nucleation through Langevin thermal fluctuations under large undercooling, formation of herringbone structures by autocatalytic growth, and microstructural evolution and transformation hysteresis in a polycrystalline alloy under uniaxial stresses. At the microscopic level we discuss new developments in phase field model of dislocation dissociation and core structure and phase field model of mislocation-a new elementary defect introduced to describe the initiation and growth of martensite. o 2006 Elsevier B. v. All rights reserved Keywords: Martensitic transformation; Phase field; Nucleation; Dislocation; Multi-scale modelin 1. Introduction formation of a critical nucleus configuration in an arbitrary pr existing microstructure and its subsequent growth without any The essential features of martensitic transformations(MTs) a priori assumptions about its shape, orientation, spatial loca- are characterized by(a) thermoelastic two-phase equilibrium tion, and arrangement of different orientation variants within that violates the Gibbs phase rule;(b) non-ergodicity that it. The conventional treatment that considers an isolated parti leads to path-dependent equilibrium microstructure and trans- cle of a given shape without capturing the effect of pre-existing formation hysteresis;(c)unique morphological patterns; and microstructures may not be sufficient to quantitatively describe (d) stress-induced transformation and shape memory effect. the nucleation and growth processes leading to self-organization These features are associated with elastic strain accommoda- of multivariant and multiphase martensitic microstructures. tion of different orientation variants of the martensitic phase in The work by Cahn [2-5] on spinodal a parent phase matrix, which dominates the transformation ther- coherent fluctuations is, in fact, the earliest application of modynamics, kinetics and crystallography. The strain-induced the phase field method to coherent transformations in solids long-range elastic interactions among the orientation variants where the transformation-induced coherency strain was consid and between them and pre-existing strain-carrying defects such ered. The extension of the method to arbitrary microstructures as dislocations, precipitates, microcracks and grain boundaries produced by diffusional and displacive transformations with determine the activation pathways for nucleation and growt arbitrary transformation strains is made possible by using the and control the overall transformation kinetics. Since the elastic microelasticity theory of Khachaturyan and Shatalov(Ks the strain energy is in general a function of size, shape, orien- ory)[1, 6, 7] who developed a reciprocal-space formulation of the tation and spatial arrangement of precipitates [1], a rigorous strainenergy as an explicit functional of arbitrary continuous dis- treatment of microstructural evolution during MTs requires a tributions of structural and/or compositional non-uniformities kinetic approach that is able to describe self-consistently the The method has been applied to various coherent phase trans- formations including MTs and many complicated strain-induced morphological patterns have been predicte Corresponding author. Tel. +1 614 292 0682: fax: +1 614 292 1537. see[8-11)). Most recently, the KS theap. ed (for recent reviews vas successfully inte- E-mail address: wang.363@osu.edu(Y. Wang). grated with the phase field models of dislocation dynamics and 0921-5093/S-see front matter
Materials Science and Engineering A 438–440 (2006) 55–63 Multi-scale phase field approach to martensitic transformations Yunzhi Wang a,∗, Armen G. Khachaturyan b a Department of Materials Science and Engineering, The Ohio State University, Columbus, OH 43210, USA b Department of Ceramic and Materials Engineering, Rutgers University, 607 Taylor Road, Piscataway, NJ 08854, USA Received 18 August 2005; received in revised form 17 March 2006; accepted 17 April 2006 Abstract Because of its flexibility in treating complex geometries and topological changes, the phase field method has been used widely in modeling microstructural evolution during various phase transformations, grain growth and, most recently, plastic deformations. We review formulations and applications of the method in the context of martensitic transformations (MTs). Examples are chosen to illustrate the capabilities of the method at both mesoscopic and microscopic length scales. At the mesoscopic level we present simulation predictions on structural configurations of critical nuclei generated by homogeneous nucleation through Langevin thermal fluctuations under large undercooling, formation of herringbone structures by autocatalytic growth, and microstructural evolution and transformation hysteresis in a polycrystalline alloy under uniaxial stresses. At the microscopic level we discuss new developments in phase field model of dislocation dissociation and core structure and phase field model of mislocation—a new elementary defect introduced to describe the initiation and growth of martensite. © 2006 Elsevier B.V. All rights reserved. Keywords: Martensitic transformation; Phase field; Nucleation; Dislocation; Multi-scale modeling 1. Introduction The essential features of martensitic transformations (MTs) are characterized by (a) thermoelastic two-phase equilibrium that violates the Gibbs phase rule; (b) non-ergodicity that leads to path-dependent equilibrium microstructure and transformation hysteresis; (c) unique morphological patterns; and (d) stress-induced transformation and shape memory effect. These features are associated with elastic strain accommodation of different orientation variants of the martensitic phase in a parent phase matrix, which dominates the transformation thermodynamics, kinetics and crystallography. The strain-induced long-range elastic interactions among the orientation variants and between them and pre-existing strain-carrying defects such as dislocations, precipitates, microcracks and grain boundaries determine the activation pathways for nucleation and growth and control the overall transformation kinetics. Since the elastic strain energy is in general a function of size, shape, orientation and spatial arrangement of precipitates [1], a rigorous treatment of microstructural evolution during MTs requires a kinetic approach that is able to describe self-consistently the ∗ Corresponding author. Tel.: +1 614 292 0682; fax: +1 614 292 1537. E-mail address: wang.363@osu.edu (Y. Wang). formation of a critical nucleus configuration in an arbitrary preexisting microstructure and its subsequent growth without any a priori assumptions about its shape, orientation, spatial location, and arrangement of different orientation variants within it. The conventional treatment that considers an isolated particle of a given shape without capturing the effect of pre-existing microstructures may not be sufficient to quantitatively describe the nucleation and growth processes leading to self-organization of multivariant and multiphase martensitic microstructures. The work by Cahn [2–5] on spinodal decomposition and coherent fluctuations is, in fact, the earliest application of the phase field method to coherent transformations in solids where the transformation-induced coherency strain was considered. The extension of the method to arbitrary microstructures produced by diffusional and displacive transformations with arbitrary transformation strains is made possible by using the microelasticity theory of Khachaturyan and Shatalov (KS theory)[1,6,7] who developed a reciprocal-space formulation of the strain energy as an explicit functional of arbitrary continuous distributions of structural and/or compositional non-uniformities. The method has been applied to various coherent phase transformations including MTs and many complicated strain-induced morphological patterns have been predicted (for recent reviews see [8–11]). Most recently, the KS theory was successfully integrated with the phase field models of dislocation dynamics and 0921-5093/$ – see front matter © 2006 Elsevier B.V. All rights reserved. doi:10.1016/j.msea.2006.04.123
Y Wang, A G Khachaturyan/Materials Science and Engineering A 438-440(2006)55-63 microcrack propagation at mesoscales [12]and with phase field with a homogeneous strain that is responsible for the martensitic model of dislocation core structures at microscales [13]. These features of the transformation advances have paved the road for realistic nano-and meso-scale tetragonal MT in a sin- for a proper fcc- bcc MT is presented as a sum of the symmetry gle crystal [14] and a more complex cubic->trigonal MT in invariants a polycrystalline system [15]. At the microscopic leve scopic phase field model of dislocation core structures [13, 161 f(n1, n2, n3= Ar discussions focus on the most recent developments of micro- 1(m2+n+n)-32(m+n+n nd its application to the study of micromechanics of nucle ation and growth of martensite[17]. It should be pointed out +A3(m+n+32 (1) that extensive work has been done at the mesoscopic level in pursuing ferroelastic and phase field approaches to martensitic where np(p=1, 2, 3)are the SOPs that describe the tetragonal transformations [18-27] and the applications discussed in this distortion of the three orientation variants along the Bain path article are just a few examples from our own work, by no means andAi(i=1, 2, 3)are the expansion coefficients. For an improper complete MT the sixth-order polynomial forming independent symmet invariants of the appropriate order has been introduced [14] 2. Phase field method at meso-scale and its applications to martensitic transformations f(m1,n2,…,m)=(m+n+…+听 Using gradient thermodynamics of non-uniform systems [28-30], the theory of microelasticity [1,6,7), and continuum A fields of conserved and non-conserved parameters, the phase m+n+…+m field method describes spatial-temporal evolution of arbitrary microstructures consisting of various types of extended defects A3(+n+… such as homo- and hetero-phase interfaces, antiphase domain boundaries, ferromagnetic and ferroelectric domain walls, and, most recently, dislocations and cracks (for the most recent 6+听吗 reviews, see [12]). A typical example of the conserved fields is +…+n2-272-1m2 concentration that characterizes chemical non-uniformity and a typical example of the non-conserved fields is the long-range (⑦m+n2+…+m) order parameter that characterizes crystal symmetry change during an order-disorder transformation. The microstructures developed in a MT can be characterized fully by a set of non- +6+吃 onserved fields, the structural order parameter(SOP)fields Different from phase field models of solidification where the where np (p=l, 2,..., n) are the SOPs that characterize the non-conserved field is introduced as a numerical technique to amplitudes of the optimal displacement modes and Ai(i=1 avoid boundary tracking, the non-conserved fields employed in 2,..., 6) are the expansion coefficients. The free energies pre- phase field models of solid-state phase transformations have sented in Eqs. (1)and(2)are specific free energies of structurall well defined physical meanings. In a proper MT such as the homogeneous finite elements with uniform values(equilibrium face centered cubic to body centered cubic ( cc- bcc) lattice or non-equilibrium) of the SOP, np. The minima of the free rearrangement in iron, for example, the SOP distinguishing the energy correspond to the equilibrium free energies of the stress- martensite and austenite phases is the tetragonal Bain distor- free parent and product phases. The minima for the product tion(a homogeneous strain that transforms an fcc lattice to a(martensite) phase are degenerate, with each of them describing bcc lattice). In an improper MT such as the cubic>tetragonal a crystallographically equivalent orientation domain transformation in Zro2 and many MTs in ferroelastic materi- In a structurally non-uniform system such as a mixture of als, the SOP is the amplitude of a"soft "optical displacement martensite and austenite phases, the finite elements characte mode that results in a mutual displacement of atoms within a unit ized by the Landau free energy have different values of np cell of the parent phase(shuffle). This primary SOP is coupled According to gradient thermodynamics [28-30], the chemical
56 Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 microcrack propagation at mesoscalses[12] and with phase field model of dislocation core structures at microscales [13]. These advances have paved the road for realistic nano- and meso-scale phase field modeling of MTs involving simultaneous plastic deformation and fracture. The latter could have important applications to transformation toughening in ceramics. This article provides an overview of the applications of the phase field methods to computer simulation of MTs at two different length scales. Thus, at the mesoscopic level, the examples include fundamental characteristics of microstructural evolution (stain-accommodating packing of martensitic variants, autocatalytic effect on nucleation and growth, and transformation hysteresis) during a generic cubic→tetragonal MT in a single crystal [14] and a more complex cubic→trigonal MT in a polycrystalline system [15]. At the microscopic level, the discussions focus on the most recent developments of microscopic phase field model of dislocation core structures [13,16] and its application to the study of micromechanims of nucleation and growth of martensite [17]. It should be pointed out that extensive work has been done at the messoscopic level in pursuing ferroelastic and phase field approaches to martensitic transformations [18–27] and the applications discussed in this article are just a few examples from our own work, by no means complete. 2. Phase field method at meso-scale and its applications to martensitic transformations Using gradient thermodynamics of non-uniform systems [28–30], the theory of microelasticity [1,6,7], and continuum fields of conserved and non-conserved parameters, the phase field method describes spatial-temporal evolution of arbitrary microstructures consisting of various types of extended defects such as homo- and hetero-phase interfaces, antiphase domain boundaries, ferromagnetic and ferroelectric domain walls, and, most recently, dislocations and cracks (for the most recent reviews, see [12]). A typical example of the conserved fields is concentration that characterizes chemical non-uniformity and a typical example of the non-conserved fields is the long-range order parameter that characterizes crystal symmetry change during an order-disorder transformation. The microstructures developed in a MT can be characterized fully by a set of nonconserved fields, the structural order parameter (SOP) fields. Different from phase field models of solidification where the non-conserved field is introduced as a numerical technique to avoid boundary tracking, the non-conserved fields employed in phase field models of solid-state phase transformations have well defined physical meanings. In a proper MT such as the face centered cubic to body centered cubic (fcc→bcc) lattice rearrangement in iron, for example, the SOP distinguishing the martensite and austenite phases is the tetragonal Bain distortion (a homogeneous strain that transforms an fcc lattice to a bcc lattice). In an improper MT such as the cubic→tetragonal transformation in ZrO2 and many MTs in ferroelastic materials, the SOP is the amplitude of a “soft” optical displacement mode that results in a mutual displacement of atoms within a unit cell of the parent phase (shuffle). This primary SOP is coupled with a homogeneous strain that is responsible for the martensitic features of the transformation. A key step in developing a phase field model is to formulate the total free energy of a system as a function of the chosen SOP fields. In the discussion of MTs, the total free energy is usually separated into two competing terms, i.e., the chemical free energy that provides the driving force for the transformation and the elastic strain energy that suppresses the transformation. The chemical free energy of a homogeneous system is usually approximated by a Landau polynomial expansion with respect to the SOPs [31–33]. For example, the simplest fourth-order polynomial approximation of the Landau free energy used [34–38] for a properfcc→bcc MT is presented as a sum of the symmetry invariants f (η1, η2, η3) = A1 2 (η2 1 + η2 2 + η2 3) − A2 3 (η3 1 + η3 2 + η3 3) + A3 4 (η2 1 + η2 2 + η2 3) 2 (1) where ηp (p = 1, 2, 3) are the SOPs that describe the tetragonal distortion of the three orientation variants along the Bain path and Ai (i = 1, 2, 3) are the expansion coefficients. For an improper MT the sixth-order polynomial forming independent symmetry invariants of the appropriate order has been introduced [14] f (η1, η2,...,ηn) = A1 2 (η2 1 + η2 2 +···+ η2 n) + A2 4 (η4 1 + η4 2 +···+ η4 n) + A3 4 (η2 1 + η2 2 +···η2 n) 2 + A4 6 (η2 1η2 2η2 3 + η2 1η2 2η2 4 +· · · + η2 n−2η2 n−1η2 n) + A5 6 (η6 1 + η6 2 +···+ η6 n) + A6 6 (η2 1 + η2 2 +···+ η2 n) 3 (2) where ηp (p = 1, 2, ..., n) are the SOPs that characterize the amplitudes of the optimal displacement modes and Ai (i = 1, 2, ..., 6) are the expansion coefficients. The free energies presented in Eqs.(1) and (2) are specific free energies of structurally homogeneous finite elements with uniform values (equilibrium or non-equilibrium) of the SOP, ηp. The minima of the free energy correspond to the equilibrium free energies of the stressfree parent and product phases. The minima for the product (martensite) phase are degenerate, with each of them describing a crystallographically equivalent orientation domain. In a structurally non-uniform system such as a mixture of martensite and austenite phases, the finite elements characterized by the Landau free energy have different values of ηp. According to gradient thermodynamics [28–30], the chemical
Y Wang, A.G. Khachaturyan/ Materials Science and Engineering A 438-440 (2006)55-63 free energy of such a system is given by energies to experimental or calculated data [43, 44]. This process also defines the length scale of the numerical simulations If the MIron. m:.. 0) +2 2A, P)V m, mo d, lattice correspondence between the parent and product phases their lattice parameters and elastic constants are known, the elas- (3) tc strain energy(4)can be formulated in rather straightforward fashion. Detailed examples can be found in [11] re Bij are the gradient energy coefficients. The first term, The spatial-temporal evolution of the SOPs, which com- pecific free energy, depends only on local values of the pletely defines the microstructural evolution during a MT, field np(r)(where r is the spatial coordinate), while the sec- obtained by solving the Onsager-type semi-phenomenological ond term, the gradient energy, accounts for contributions from kinetic equations of motion, which assume a linear dependence spatial variation of np(r). The interplay between the two deter- of the rate of evolution, anp/at, on the driving force, 8 F/6np mines the equilibrium profiles of np and hence the widths and energies of interfaces between different orientation variants of the martensitic phase and between the martensite and parer 9=l ong(r, t +sp(r, t) To remove the structural incompatibility between adjacent finite elements of different values of SOP, one need to introduce where F=Fch +Eel is the total free energy of the system,with additional inhomogeneous displacements providing the continu- Fcn being the chemical free energy and e the elastic energy ity of the total displacement field( the crystal lattice coherency). Lpg are the kinetic coefficients and 5p is the Langevin random By definition, this is an elastic displacement field that provides force term that describes thermal fluctuations [31,45-471 the elastic strain energy. According to the Ks theory [1, 6,7] The phase field method formulated above offers a self- the elastic strain energy for arbitrary structural non-uniformities consistent treatment of the thermodynamics and kinetics of MTs characterized by np(r)in an elastically anisotropic crystal under involving arbitrary multivariant configuration and particle mor- the homogeneous modulus assumption is given by an explicit phology at mesoscopic length scales. The effect of long-range elastic interactions on the initiation and growth of martensite is taken into account automatically by including the elastic strain ∑+8m(7) (4 energy in the total free energy in Eq (6). The models have been (4) applied successfully to proper and improper MTs in single crys- where Inp(r))g is the Fourier transform of the function np(r) that tals [14,37], polycrystalline alloys [15, 48), multi-layer systems [49], and thin-films [50] and the numerical simulations have characterizes an arbitrary structural non-uniformity of the pth type(in principle, the structural non-uniformities could be asso- Shed light on the micromechanisms underlying microstructural ciated with any types of extended crystal defects such as coherent development during MTs One of the interesting observations from the phase field sim precipitate, dislocations, grain boundaries, microcracks, etc. ),g ulations is the formation of multivariant polytwinned embryos represents an arbitrary point in the reciprocal space, e=g/g, g through homogeneous nucleation under large undercooling con- indicates complex conjugate, m=l for a proper MT [37] and ditions. Fig. I shows an example of the phase field simulation of m=2 for an improper MT[14], and an improper cubic-tetragonal MT in an elastically Bpg(e)=CKIE (P)e&(q)-e00(P)2 (e)ogr(q)er (5) single crystal with the SFTS being a pure shear [14. The where Cijkl are the elastic constants, e!(P)is the stress-free trans- strain energy, GEt, and the chemical driving force, Af(D,i.e formation strain(SFTS)of type p martensite variant, o(p)= 5=GE0/Af(T), where G is the typical shear modulus, Eo is the CiReR (p), and 2*(e)=Cike; e is the inverse of the Green's typical SFTs, and a/D) is the ditterence of the specific chemical free energy between the martensite and parent phases. This ratio function in the reciprocal space. f in Eq (4)represents the prin- was chosen as 0.056 to mimic a large undercooling(high driving ciple value of the integral that excludes a small volume in the force)condition. The three orientation variants were character reciprocal space.(21)/, at g=0(V is the total volume of the ized by three SOP fields and fi(ul, m2, ..,m)=f(n, n2, n3)in Eq (2). To visualize clearly a homogeneous nucleation event and 3. For a given MT, the symmetry invariants of the SOPs in configurations of critical or operational nuclei, only two orienta Landau free energy can be derived by the symmetry of tion variants were considered. They are represented in Fig. I by the co-existing phases [31-33] and the expansion coefficients the bright and dark shades, respectively. The parent phase is rep- of a Landau polynomial can be determined by fitting the Lan- resented by a gray background. The nine small squares presente dau free energy to thermodynamic databases or first principles in each micrograph are the consecutive equally spaced (010) calculations [ 39, 40](for recent reviews see 35, 36]). Ther re are cross sections of a three-dimensional (3D) cubic computational increasing efforts in calculating the gradient energy coefficients cell with 643 mesh points and a mesh size of 1.0nm. The initial for various types of interfaces from first principles [41, 42]. If condition is an"as-quenched"homogeneous cubic phase that is such data are not available for a particular system, the gradi- in a metastable state. Since no other crystal defects were con- ent energy coefficients can be determined by fitting interfacial sidered, the transformation developed through a homogeneous
Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 57 free energy of such a system is given by Fch = V ⎡ ⎣f (η1, η2,...,ηn) + 1 2 n p=1 βij(p)∇iηp∇jηp ⎤ ⎦d3r (3) where βij are the gradient energy coefficients. The first term, the specific free energy, depends only on local values of the field ηp(r) (where r is the spatial coordinate), while the second term, the gradient energy, accounts for contributions from spatial variation of ηp(r). The interplay between the two determines the equilibrium profiles of ηp and hence the widths and energies of interfaces between different orientation variants of the martensitic phase and between the martensite and parent phases. To remove the structural incompatibility between adjacent finite elements of different values of SOP, one need to introduce additional inhomogeneous displacements providing the continuity of the total displacement field (the crystal lattice coherency). By definition, this is an elastic displacement field that provides the elastic strain energy. According to the KS theory [1,6,7], the elastic strain energy for arbitrary structural non-uniformities characterized by ηp(r) in an elastically anisotropic crystal under the homogeneous modulus assumption is given by an explicit close form (4) where {ηp(r)}g is the Fourier transform of the function ηp(r) that characterizes an arbitrary structural non-uniformity of the pth type (in principle, the structural non-uniformities could be associated with any types of extended crystal defects such as coherent precipitate, dislocations, grain boundaries, microcracks, etc.), g represents an arbitrary point in the reciprocal space, e = g/g, “*” indicates complex conjugate, m = 1 for a proper MT [37] and m = 2 for an improper MT [14], and Bpq(e) ≡ Cijklε0 ij(p)ε0 kl(q) − eiσ0 ij(p)Ωjk(e)σ0 kl(q)el (5) whereCijkl are the elastic constants, ε0 ij(p) is the stress-free transformation strain (SFTS) of type p martensite variant, σ0 ij(p) ≡ Cijklε0 kl(p), and Ω−1 jk (e) = Cijkleiel is the inverse of the Green’s function in the reciprocal space. in Eq. (4) represents the principle value of the integral that excludes a small volume in the reciprocal space, (2π) 3/V, at g =0(V is the total volume of the system). For a given MT, the symmetry invariants of the SOPs in the Landau free energy can be derived by the symmetry of the co-existing phases [31–33] and the expansion coefficients of a Landau polynomial can be determined by fitting the Landau free energy to thermodynamic databases or first principles calculations [39,40] (for recent reviews see [35,36]). There are increasing efforts in calculating the gradient energy coefficients for various types of interfaces from first principles [41,42]. If such data are not available for a particular system, the gradient energy coefficients can be determined by fitting interfacial energies to experimental or calculated data [43,44]. This process also defines the length scale of the numerical simulations. If the lattice correspondence between the parent and product phases, their lattice parameters and elastic constants are known, the elastic strain energy (4) can be formulated in a rather straightforward fashion. Detailed examples can be found in [11]. The spatial-temporal evolution of the SOPs, which completely defines the microstructural evolution during a MT, is obtained by solving the Onsager-type semi-phenomenological kinetic equations of motion, which assume a linear dependence of the rate of evolution, ∂ηp/∂t, on the driving force, F/ηp, ∂ηp(r, t) ∂t = − N q=1 Lpq δF δηq(r, t) + ξp(r, t) (6) where F = Fch + Eel is the total free energy of the system, with Fch being the chemical free energy and Eel the elastic energy, Lpq are the kinetic coefficients and ξp is the Langevin random force term that describes thermal fluctuations [31,45–47]. The phase field method formulated above offers a selfconsistent treatment of the thermodynamics and kinetics of MTs involving arbitrary multivariant configuration and particle morphology at mesoscopic length scales. The effect of long-range elastic interactions on the initiation and growth of martensite is taken into account automatically by including the elastic strain energy in the total free energy in Eq. (6). The models have been applied successfully to proper and improper MTs in single crystals [14,37], polycrystalline alloys [15,48], multi-layer systems [49], and thin-films [50] and the numerical simulations have shed light on the micromechanisms underlying microstructural development during MTs. One of the interesting observations from the phase field simulations is the formation of multivariant polytwinned embryos through homogeneous nucleation under large undercooling conditions. Fig. 1 shows an example of the phase field simulation of an improper cubic→tetragonal MT in an elastically isotropic single crystal with the SFTS being a pure shear [14]. The “strength” of the MT is characterized by the ratio of the typical strain energy, Gε2 0, and the chemical driving force, f(T), i.e., ζ = Gε2 0/f (T ), where G is the typical shear modulus, ε0 is the typical SFTS, and f(T) is the difference of the specific chemical free energy between the martensite and parent phases. This ratio was chosen as 0.056 to mimic a large undercooling (high driving force) condition. The three orientation variants were characterized by three SOP fields and f(η1, η2, ..., ηn) = f(η1, η2, η3) in Eq.(2). To visualize clearly a homogeneous nucleation event and configurations of critical or operational nuclei, only two orientation variants were considered. They are represented in Fig. 1 by the bright and dark shades, respectively. The parent phase is represented by a gray background. The nine small squares presented in each micrograph are the consecutive equally spaced (0 1 0) cross sections of a three-dimensional (3D) cubic computational cell with 643 mesh points and a mesh size of 1.0 nm. The initial condition is an “as-quenched” homogeneous cubic phase that is in a metastable state. Since no other crystal defects were considered, the transformation developed through a homogeneous
Y Wang, A G Khachaturyan/Materials Science and Engineering A 438-440(2006)55-63 A N Fig. 1. Microstructural development during a cubic-tetragonal martensitic transformation through homogeneous nucleation simulated by the phase field method 14). The nine small squires in each micrograph are the consecutive 2D cross sections of a 3D cube along the [0 1 0] axis. (A-D)Correspond to reduced time =2, 6. nucleation process simulated by the Langevin random force term three orientation variants form initially an internally twinned given in Eq. (6). No a priori assumptions about possible crit- martensitic platelet( Fig. 2 at [=2), the third orientation variant ical nucleus configurations were made. The simulation result nucleates spontaneously at the interfaces between the matrix and presented in Fig. 1(A)shows that the stochastic random noises the martensitic platelet(Fig. 2 at [=5). The growth of the third produce critical nuclei consisting of two twin-related domains. variant induces the outgrowth of one of the two variants in the These compound nuclei were formed by either a collective pro- existing martensitic platelet, forming two new internally twined cess or a correlated process assisted by the autocatalytic effect platelets, one on each side of the original martensitic platelet discussed in [51]. Such an internally twinned structure of the(Fig. 2 at t=7). Recurring of this process results in the herring embryos reduces considerably the strain energy [l](see also bone structure consisting of adjacent internally twinned plates Fig. 7 in Section 3). This allows us to assume safely that het -(Fig. 2 from [=9 to T= 13). The herringbone structure was also erogeneous nucleation on lattice defects should also produce predicted for the cubic-trigonal proper MT[15]. These pre compound nuclei of polytwinned structures dictions agree well with experimental observations. The growth process of the polytwinned nuclei(Fig. 1(B One of the most complicated MTs that have been studied by and(C)is highly anisotropic, with the alternating twin-related the phase field method is the cubic- trigonal proper MT in a domains mostly expanding in directions parallel to their 110 polycrystalline Au-Cd alloy [15]. The trigonal lattice of the 5? habit planes. The growing martensitic particles have basically a martensite in Au-Cd can be visualized as a stretched cubic lattice lenticular shape before they finally joined to form two intersect- in one of the body diagonal (i.e, [11 1]) directions. Four lattice ing internally twinned thin plates of the invariant plane habits correspondence variants are associated with the transformation When all three variants were considered, a herringbone struc- the phase field model, the spatial distribution of the four vari- ture developed by self-assembly of the three variants(rep- ants is characterized by four SOPs and the chemical free energy resented by different shades of gray in Fig. 2)during the is approximated by the fourth-order Landau expansion polyno- cubic-tetragonal MT. It was found that autocatalysis plays an mial presented in Eq (1). Eight randomly oriented grains were important role in the self-assembly process during growth which considered in the polycrystalline system(Fig 3). To present the leads to the herringbone structure. For example, when two of the SFTS in a global coordinate system, a rotation operation was
58 Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 Fig. 1. Microstructural development during a cubic→tetragonal martensitic transformation through homogeneous nucleation simulated by the phase field method [14]. The nine small squires in each micrograph are the consecutive 2D cross sections of a 3D cube along the [0 1 0] axis. (A–D) Correspond to reduced time = 2, 6, 10 and 20. nucleation process simulated by the Langevin random force term given in Eq. (6). No a priori assumptions about possible critical nucleus configurations were made. The simulation result presented in Fig. 1(A) shows that the stochastic random noises produce critical nuclei consisting of two twin-related domains. These compound nuclei were formed by either a collective process or a correlated process assisted by the autocatalytic effect discussed in [51]. Such an internally twinned structure of the embryos reduces considerably the strain energy [1] (see also Fig. 7 in Section 3). This allows us to assume safely that heterogeneous nucleation on lattice defects should also produce compound nuclei of polytwinned structures. The growth process of the polytwinned nuclei (Fig. 1(B) and (C)) is highly anisotropic, with the alternating twin-related domains mostly expanding in directions parallel to their {110} habit planes. The growing martensitic particles have basically a lenticular shape before they finally joined to form two intersecting internally twinned thin plates of the invariant plane habits (Fig. 1(D)). When all three variants were considered, a herringbone structure developed by self-assembly of the three variants (represented by different shades of gray in Fig. 2) during the cubic→tetragonal MT. It was found that autocatalysis plays an important role in the self-assembly process during growth which leads to the herringbone structure. For example, when two of the three orientation variants form initially an internally twinned martensitic platelet (Fig. 2 at τ = 2), the third orientation variant nucleates spontaneously at the interfaces between the matrix and the martensitic platelet (Fig. 2 at τ = 5). The growth of the third variant induces the outgrowth of one of the two variants in the existing martensitic platelet, forming two new internally twined platelets, one on each side of the original martensitic platelet (Fig. 2 at τ = 7). Recurring of this process results in the herringbone structure consisting of adjacent internally twinned plates (Fig. 2 from τ = 9 to τ = 13). The herringbone structure was also predicted for the cubic→trigonal proper MT [15]. These predictions agree well with experimental observations. One of the most complicated MTs that have been studied by the phase field method is the cubic→trigonal proper MT in a polycrystalline Au–Cd alloy [15]. The trigonal lattice of the ζ 2 martensite in Au–Cd can be visualized as a stretched cubic lattice in one of the body diagonal (i.e., [1 1 1]) directions. Four lattice correspondence variants are associated with the transformation, which correspond to the four 111 directions of the cube. In the phase field model, the spatial distribution of the four variants is characterized by four SOPs and the chemical free energy is approximated by the fourth-order Landau expansion polynomial presented in Eq. (1). Eight randomly oriented grains were considered in the polycrystalline system (Fig. 3). To present the SFTS in a global coordinate system, a rotation operation was
Y Wang, A.G. Khachaturyan/ Materials Science and Engineering A 438-440 (2006)55-63 T 5 IT 自=最自 Fig. 2. Formation of herringbone structure through autocatalytic growth during a cubic- tetragonal martensitic transformation. The nine small squires in each micrograph are the consecutive 2D cross sections of a 3D cube along the [0 1 0] axis. t is reduced time. applied to the SftS derived for each grain within each grain but differs from one grain to another. Fig. 4 shows the microstructural evolution obtained under external uni- ey (r)=Rik()rj(r)eu(r). (7) axial stresses in a system of 1283 mesh points and a mesh size where Ri (r) is a 3 x 3 matrix that defines the orientation of the of 0.5 pm. The strength parameter of the MT, s, is chosen to grain in the global coordinate system. It has a constant value be 5.0, which corresponds to a small undercooling. The four orientation variants are represented by four different shades of gray in the figure(color online). The multivariant microstru tures observed in the polycrystalline system is found to be quite different from the one observed in a single crystal. Because of the elastic coupling between neighboring randomly oriented par tially transformed grains, the MT in the polycrystalline system did not go to completion and the multi-domain structure is sta- ble against further growth, which is contrary to the simulation results obtained in a single crystal where the mt went to com- pletion under exactly the same conditions. This difference is caused by the geometrical constraints imposed on the mt in a polycrystalline system. The stress-strain hysteresis correspond ing to the microstructures under different uniaxial stresses also shown in Fig. 4. The nucleation of new variants and the domain boundary movement is clearly reproduced in the simu- lation. This example demonstrates well the potential of the phase field method in predicting very complex strain accommodating assemblages of multiple orientation domains produced by mts in polycrystalline materials under applied stresses. 3. Microscopic phase field model of dislocation core structures and its applications to martensitic transformations Polycrystal structure of the parent phase with eight randomly oriented While the mesoscopic phase field model of MT has achieved remarkable success in predicting stain-accommodating packing
Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 59 Fig. 2. Formation of herringbone structure through autocatalytic growth during a cubic→tetragonal martensitic transformation. The nine small squires in each micrograph are the consecutive 2D cross sections of a 3D cube along the [0 1 0] axis. τ is reduced time. applied to the SFTS derived for each grain, ε 0,g ij (r) = Rik(r)Rjl(r)ε0 ij(r), (7) where Rij(r) is a 3 × 3 matrix that defines the orientation of the grain in the global coordinate system. It has a constant value Fig. 3. Polycrystal structure of the parent phase with eight randomly oriented grains in the computational volume. within each grain but differs from one grain to another. Fig. 4 shows the microstructural evolution obtained under external uniaxial stresses in a system of 1283 mesh points and a mesh size of 0.5m. The strength parameter of the MT, ζ, is chosen to be 5.0, which corresponds to a small undercooling. The four orientation variants are represented by four different shades of gray in the figure (color online). The multivariant microstructures observed in the polycrystalline system is found to be quite different from the one observed in a single crystal. Because of the elastic coupling between neighboring randomly oriented partially transformed grains, the MT in the polycrystalline system did not go to completion and the multi-domain structure is stable against further growth, which is contrary to the simulation results obtained in a single crystal where the MT went to completion under exactly the same conditions. This difference is caused by the geometrical constraints imposed on the MT in a polycrystalline system. The stress–strain hysteresis corresponding to the microstructures under different uniaxial stresses is also shown in Fig. 4. The nucleation of new variants and the domain boundary movement is clearly reproduced in the simulation. This example demonstrates well the potential of the phase field method in predicting very complex strain accommodating assemblages of multiple orientation domains produced by MTs in polycrystalline materials under applied stresses. 3. Microscopic phase field model of dislocation core structures and its applications to martensitic transformations While the mesoscopic phase field model of MT has achieved remarkable success in predicting stain-accommodating packing
Y Wang, A G Khachaturyan/Materials Science and Engineering A 438-440(2006)55-6 Reloading O/G Martensitic variant 1, with the trigonal axis along Martensitic variant 3, with the trigonal axis along Grain boundary Fig. 4. The hysteresis loop and the 3D microstructures obtained at different stresses for a cubic- trigonal martensitic transformation in a polycrystalline system 15 of martensitic variants, autocatalytic effect, and transformation faults and grain boundaries [36, 53-59]. The strain fields assoc hysteresis, it offers little knowledge about the heterogeneous ated with the martensitic particles may be partially or completely processes occurring at the dislocation level. Even though homo- cancelled by the strain fields generated by the lattice defects. geneous nucleation of martensite through the formation of mul- This would lower significantly or eliminate completely the acti- tivariant polytwinned embryos under large undercooling has vation barriers of the kinetic pathways of nucleation and growth been demonstrated in the phase field simulations and homo- Therefore, it is essential to include dislocation-level activities geneous nucleation of martensite has been observed in small in models of MTs. The recent development of the phase field particle experiments [52], most MTs occur through heteroge- approach to dislocation dynamics has offered a unique oppor- neous nucleation at lattice defects such as dislocations, stacking tunity to treat rigorously and self-consistently heterogeneous
60 Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 Fig. 4. The hysteresis loop and the 3D microstructures obtained at different stresses for a cubic→trigonal martensitic transformation in a polycrystalline system [15]. of martensitic variants, autocatalytic effect, and transformation hysteresis, it offers little knowledge about the heterogeneous processes occurring at the dislocation level. Even though homogeneous nucleation of martensite through the formation of multivariant polytwinned embryos under large undercooling has been demonstrated in the phase field simulations and homogeneous nucleation of martensite has been observed in small particle experiments [52], most MTs occur through heterogeneous nucleation at lattice defects such as dislocations, stacking faults and grain boundaries [36,53–59]. The strain fields associated with the martensitic particles may be partially or completely cancelled by the strain fields generated by the lattice defects. This would lower significantly or eliminate completely the activation barriers of the kinetic pathways of nucleation and growth. Therefore, it is essential to include dislocation-level activities in models of MTs. The recent development of the phase field approach to dislocation dynamics has offered a unique opportunity to treat rigorously and self-consistently heterogeneous
Y Wang, A.G. Khachaturyan/ Materials Science and Engineering A 438-440 (2006)55-63 Fig. 5. Time-evolution of dislocation substructures on a(111) plane of an fcc crystal during annealing simulated by the phase field method [13] nucleation of martensite on pre-existing dislocations and grain term that is proportional only to the dislocation line length and boundaries within a single framework. describes the effective dislocation core energy y treating a dislocation loop as a thin platelet misfitting inclusion(e.g, a thin martensitic platelet of a single variant) sas eing formulated in the phase field framework, the model able to describe collective motion of dislocations of arbi a phase field description of the spatial-temporal evolution of trary configurations and dislocation-precipitate interactions at gliding dislocations was developed [60]. In this approach a new meso-scales. Topological changes such as nucleation, multipli set of sops is introduced to characterize the structural non- cation annihilation and reaction of dislocations are accounted uniformities associated with dislocations. A region enclosed by for naturally without explicitly tracking the moving dislocation a dislocation loop on a slip plane can be regarded as a"trans- lines(see, e.g., Fig. 5(13). To apply the model to study the formed region"that has been plastically deformed by dislocation micromechanisms of MTs, however, one needs to resolve the glide and the boundaries between the transformed regions of dif- details of dislocation core structures because dissociation of lat ferent type and number of slips are lines of dislocations. These tice dislocations is essential in dislocation models of martensite slipped regions on each individual slip plane are characterized embryos [54-59. Recently, a microscopic phase field model by the SOPs, n(a, ma, r), where, a and ma index the slip plane of dislocation dissociation and core structures [13, 16] has been and slip direction, respectively. The number of the structural developed, which employs ab initio GSF energy as the model order parameters required equals to the number of operative slip input. It has been shown quantitatively systems in a crystal. field dislocation model is a 3D generalization of the Peierls- The time-evolution of the dislocation loops is treated in a sim- Nabarro(P-N) model [62, 63]. When applied to straight dislo- ilar way as how the evolution of martensitic particles is described cations, a complete agreement of the phase field model with in the phase field model introduced above, e.g., by Eq (6). Simi- the P-N model for core structures [64] has been achieved using lar to the energetics of phase field model of MT discussed earlier, the same set of ab initio data of GSF energies [65](Fig. 6) the total energy of a dislocation system consists of three terms the crystalline energy that replaces the local specific chemical free energy, the gradient energy, and the elastic strain energy. The crystalline energy is a periodic energy landscape associ- ated with a general plastic deformation in a crystal by arbitrary o linear combinations of localized simple shears(slips)associ- ated with all operative slip systems [13]. when projected onto a particular slip plane, the potential energy landscape reduces to 0. 6- n(r) the so-called generalized stacking fault(GSF)energy [61]. The elastic energy equation is identical to the one formulated for 0. 4 MT(e.g, Eq(4)), with the SFTS of martensite replaced by the 0.3 eigenstrain of a dislocation loop. The gradient energy accounts dn(x) for contributions from spatial non-uniformity of n(a, ma, r)in the slip plane(inhomogeneity in the slip displacement). To take 0.1) into account the fact that the crystal lattice is the same on both sides of the slip plane and thus the slip plane does not introduce interfacial energy, the gradient terms have been formulated [60] in such a form that their values are finite only at the disloc- Fig. 6. Quantitative comparison of the core structures of an edge dislocation in Al calculated by the phase field model (lines)[ 16] and the Peierls model (poin tion line and vanish at the slip plane. This results in an energy [64] with the same GSF energy [65]
Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 61 Fig. 5. Time-evolution of dislocation substructures on a (1 1 1) plane of an fcc crystal during annealing simulated by the phase field method [13]. nucleation of martensite on pre-existing dislocations and grain boundaries within a single framework. By treating a dislocation loop as a thin platelet misfitting inclusion (e.g., a thin martensitic platelet of a single variant), a phase field description of the spatial-temporal evolution of gliding dislocations was developed [60]. In this approach a new set of SOPs is introduced to characterize the structural nonuniformities associated with dislocations. A region enclosed by a dislocation loop on a slip plane can be regarded as a “transformed region” that has been plastically deformed by dislocation glide and the boundaries between the transformed regions of different type and number of slips are lines of dislocations. These slipped regions on each individual slip plane are characterized by the SOPs, η(α, m, r), where, α and m index the slip plane and slip direction, respectively. The number of the structural order parameters required equals to the number of operative slip systems in a crystal. The time-evolution of the dislocation loops is treated in a similar way as how the evolution of martensitic particles is described in the phase field model introduced above, e.g., by Eq. (6). Similar to the energetics of phase field model of MT discussed earlier, the total energy of a dislocation system consists of three terms: the crystalline energy that replaces the local specific chemical free energy, the gradient energy, and the elastic strain energy. The crystalline energy is a periodic energy landscape associated with a general plastic deformation in a crystal by arbitrary linear combinations of localized simple shears (slips) associated with all operative slip systems [13]. When projected onto a particular slip plane, the potential energy landscape reduces to the so-called generalized stacking fault (GSF) energy [61]. The elastic energy equation is identical to the one formulated for MT (e.g, Eq. (4)), with the SFTS of martensite replaced by the eigenstrain of a dislocation loop. The gradient energy accounts for contributions from spatial non-uniformity of η(α, m, r) in the slip plane (inhomogeneity in the slip displacement). To take into account the fact that the crystal lattice is the same on both sides of the slip plane and thus the slip plane does not introduce interfacial energy, the gradient terms have been formulated [60] in such a form that their values are finite only at the dislocation line and vanish at the slip plane. This results in an energy term that is proportional only to the dislocation line length and describes the effective dislocation core energy. Being formulated in the phase field framework, the model is able to describe collective motion of dislocations of arbitrary configurations and dislocation-precipitate interactions at meso-scales. Topological changes such as nucleation, multiplication, annihilation and reaction of dislocations are accounted for naturally without explicitly tracking the moving dislocation lines (see, e.g., Fig. 5 [13]). To apply the model to study the micromechanisms of MTs, however, one needs to resolve the details of dislocation core structures because dissociation of lattice dislocations is essential in dislocation models of martensite embryos [54–59]. Recently, a microscopic phase field model of dislocation dissociation and core structures [13,16] has been developed, which employs ab initio GSF energy as the model input. It has been shown quantitatively [13,16] that the phase field dislocation model is a 3D generalization of the PeierlsNabarro (P-N) model [62,63]. When applied to straight dislocations, a complete agreement of the phase field model with the P-N model for core structures [64] has been achieved using the same set of ab initio data of GSF energies [65] (Fig. 6). Fig. 6. Quantitative comparison of the core structures of an edge dislocation in Al calculated by the phase field model (lines) [16] and the Peierls model (points) [64] with the same GSF energy [65]
Y Wang, A G Khachaturyan/Materials Science and Engineering A 438-440(2006)55-63 The microscopic phase field model has been applied to study the energy and sliding resistance of Peierls grain boundaries (small angle grain boundaries consisting of regular dislocation networks)[16] as a function of misorientation. It has also been applied to study the shearing of y precipitates[66]in an effort to +Layer-1 understand the effect of microstructural characteristics on defor- (variant 1) o For a sinmple fcc-hcp MT, the microscopic phase field model ation mechanisms observed in Ni-based superalloy 12 of dislocations with ab initio data of the GSF energy is bein applied directly to study the nucleation mechanisms associated with dissociation of a group of pre-existing lattice dislocations as suggested by Olson and Cohen [54]. Fo (variant 2) r more co MTs such as the fcc-bcc lattice rearrangment, however, the faulting mechanisms proposed for the formation of a marten- volume site embryo involve multiple sets of dissociated dislocations distributed among multiple adjacent atomic planes [55]. While ig. 3. Relaxed shapes of mi ocapon oops at iteren ixed vo umes tod a scrutiny of atomistic simulations, more straightforward descrip tions have been proposed [17](a 2D attempt using the Element Free-Galerkin method can be found in (59). In particular, a new Bain path as model inputs. The elastic energy of the mislocation elementary defect at the atomic scale called mislocation was is calculated using the KS theory [1,6,7]. The total energies of introduced [17. A mislocation is defined as the smallest ele eneous (single variant) and a heterogeneous(two twin- mentary defect for MTs and further decomposition of it into a related variants) two-layer fault of the Bain mislocations are multiple set of dislocations is unnecessary. Forexample, the Bain shown in Fig. 7. It can be seen clearly that the activation energy for the formation of an internally twinned embryo is much lower listortion could be regarded as a mislocation of the fcc- b than that of a single variant embryo. The relaxed shapes of transformation whose core contains both dilatational and shear strain components. The concept of mislocations may provide a the mislocation loops at fixed volumes for the heterogeneous powerful way of describing martensite nucleation, growth and two-layer fault are shown in Fig. 8, which seems to be dif impingement using the simple laws of interactions and reactions ferent from the oblate spheroidal embryo assumed in literature between these elementary defects The core profile of a mislocation, the activation barrier of the minimum energy pathway, and the morphology of a critical 4 Summary nucleus consisting of mislocations have been investigated [17] by using the microscopic phase field model [13, 16], with ab Phase field modeling capabilities developed for marten- tio calculations of the crystalline energy corresponding to the sitic transformations at multiple length scales are reviewed. At the mesoscopic length scales, the models are shown to be able to describe arbitrary multivariant and multiphase strain- accommodating morphological patterns produced by marten- sitic transformations of arbitrary stress-free transformation strains without any a priori assumptions on the transforma- tion paths. Homogeneous nucleation under large undercooling collective process or a correlated process assisted by autocatal- ysis. The autocatalytic effect also plays an important role in the rowth process leading to a herringbone structure consisting of djacent internally twinned plates of invariant plane habits. The models ability to describe martensitic transformations in a poly- crystalline material under external stresses is also demonstrated At the microscopic level, the newly developed phase field model of dislocation core structure and phase field model of miso- 20253035 cation allow for quantitative characterization of the minimum energy pathways and critical nucleus configurations with state- of-the-art ab initio and atomistic calculations as inputs. These Fig.7. Total energy of a homogeneous(single variant)(+)and a heterogeneous multi-scale modeling capabilities developed within a common loops calculated by the microscopic phase field method [171. Here u is shear phase field framework could offer an opportunity to develop modulus, d is the interplanar distance of (110)twin plane. The effective radius unprecedented new understanding of martensitic transforma- is given as R=Vv/ad, where Vis the volume of the nucleus tons
62 Y. Wang, A.G. Khachaturyan / Materials Science and Engineering A 438–440 (2006) 55–63 The microscopic phase field model has been applied to study the energy and sliding resistance of Peierls grain boundaries (small angle grain boundaries consisting of regular dislocation networks) [16] as a function of misorientation. It has also been applied to study the shearing of γ precipitates[66] in an effort to understand the effect of microstructural characteristics on deformation mechanisms observed in Ni-based superalloys. For a simple fcc–hcp MT, the microscopic phase field model of dislocations with ab initio data of the GSF energy is being applied directly to study the nucleation mechanisms associated with dissociation of a group of pre-existing lattice dislocations as suggested by Olson and Cohen [54]. For more complicated MTs such as the fcc–bcc lattice rearranegment, however, the faulting mechanisms proposed for the formation of a martensite embryo involve multiple sets of dissociated dislocations distributed among multiple adjacent atomic planes [55]. While the activation energy of such a faulting pathway is awaiting for scrutiny of atomistic simulations, more straightforward descriptions have been proposed [17] (a 2D attempt using the ElementFree-Galerkin method can be found in [59]). In particular, a new elementary defect at the atomic scale called mislocation was introduced [17]. A mislocation is defined as the smallest elementary defect for MTs and further decomposition of it into a multiple set of dislocations is unnecessary. For example, the Bain distortion could be regarded as a mislocation of the fcc→bcc transformation whose core contains both dilatational and shear strain components. The concept of mislocations may provide a powerful way of describing martensite nucleation, growth and impingement using the simple laws of interactions and reactions between these elementary defects. The core profile of a mislocation, the activation barrier of the minimum energy pathway, and the morphology of a critical nucleus consisting of mislocations have been investigated [17] by using the microscopic phase field model [13,16], with ab initio calculations of the crystalline energy corresponding to the Fig. 7. Total energy of a homogeneous (single variant) (+) and a heterogeneous (two twin-related variants) (×) two-layer fault consisting of Bain mislocation loops calculated by the microscopic phase field method [17]. Here μ is shear modulus, d is the interplanar distance of (110) twin plane. The effective radius ¯ is given as R = V/πd, where V is the volume of the nucleus. Fig. 8. Relaxed shapes of mislocation loops at different fixed volumes for a heterogeneous two-layer fault simulated by the microscopic phase field model [17]. Bain path as model inputs. The elastic energy of the mislocation is calculated using the KS theory [1,6,7]. The total energies of a homogeneous (single variant) and a heterogeneous (two twinrelated variants) two-layer fault of the Bain mislocations are shown in Fig. 7. It can be seen clearly that the activation energy for the formation of an internally twinned embryo is much lower than that of a single variant embryo. The relaxed shapes of the mislocation loops at fixed volumes for the heterogeneous two-layer fault are shown in Fig. 8, which seems to be different from the oblate spheroidal embryo assumed in literature [67]. 4. Summary Phase field modeling capabilities developed for martensitic transformations at multiple length scales are reviewed. At the mesoscopic length scales, the models are shown to be able to describe arbitrary multivariant and multiphase strainaccommodating morphological patterns produced by martensitic transformations of arbitrary stress-free transformation strains without any a priori assumptions on the transformation paths. Homogeneous nucleation under large undercooling generates multivariant polytwinned embryos through either a collective process or a correlated process assisted by autocatalysis. The autocatalytic effect also plays an important role in the growth process leading to a herringbone structure consisting of adjacent internally twinned plates of invariant plane habits. The model’s ability to describe martensitic transformations in a polycrystalline material under external stresses is also demonstrated. At the microscopic level, the newly developed phase field model of dislocation core structure and phase field model of mislocation allow for quantitative characterization of the minimum energy pathways and critical nucleus configurations with stateof-the-art ab initio and atomistic calculations as inputs. These multi-scale modeling capabilities developed within a common phase field framework could offer an opportunity to develop unprecedented new understanding of martensitic transformations
Y Wang, A.G. Khachaturyan/ Materials Science and Engineering A 438-440 (2006)55-63 Acknowledgements [27] V.I. Levitas, D L. Preston, Phys. Lett. A 343(2005)32 [28]JS Rowlinson, J. Stat. Phys. 20(1979)198. e The work is supported by the Office of Naval Research(ONR)[29]JWCahn,JE.Hilliard,J.Chem.Phys.28(1958)258-267 der grant No0014-05-1-0504 (Y W) and the National Science [30] M. Hillert, Acta Metall. 9(1961)525. Foundation(NSF)under grant DMR-0139705 (YW)and grant [31] E.M. Lifshitz, L P. Pitaevskii, Part 1, Landau and Lifshitz Course of The. DMR-0242619(AK). We thank Prof J. Li and Dr C. Shen at [32] Y.A. Izyumov, V.N. Syromoyatnikov, Phase Transitions and Crystal Sym- the Ohio State University for their valuable comments on the metry, Kluwer Academic Publishers, Boston, 1990 manuscripts [33] P. Toledano, V Dmitriev, Reconstructive Phase Transitions, World Scien tific, New Jersey. 1996. [34]R. Bruinsma, A Zangwill, J Phys. 47(1986)2055-207 References [35]G B. Olson, Mater. Sci. Eng. 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